WU Lina,SUN Congjian,HE Qiang,et al.Analysis of Temporal and Spatial Variation of Hydrochemical Characteristics of the Typical Inland River in the Middle of Tianshan Mountains[J].Research of Soil and Water Conservation,2017,24(05):149-156.
中天山典型内陆河流域水化学时空特征分析
- Title:
- Analysis of Temporal and Spatial Variation of Hydrochemical Characteristics of the Typical Inland River in the Middle of Tianshan Mountains
- Keywords:
- Urumqi River; temporal and spatial distribution; Piper; gibbs; control factors
- 分类号:
- S153;P332.7
- 摘要:
- 基于2011—2013年不同季节乌鲁木齐河流域6个站点52组地表水化学的测试结果，结合流域气象水文资料，利用水化学分析方法和SPSS统计软件分析了乌鲁木齐河流域地表水化学时空变化特征、地表水各离子间相关性以及流域水化学特征的控制因素。结果表明：（1）乌鲁木齐河流域地表水总体矿化度较低，水体呈弱碱性。（2）流域地表水化学具有明显的季节变化趋势即早春融雪季、春末夏初季和秋季融雪季TDS值偏高，夏季TDS值低；同时也表现出较明显的年际差异性：多雨的年份地表水TDS值较低，少雨的年份地表水TDS值较高。（3）控制地表水体的主要离子为HCO3-，Ca2+，SO42-，离子质量浓度大小依次为HCO3- > Ca2+ > SO42- > Cl- > Na+ > Mg2+ > K+ > CO32-；不同季节控制水体的主要离子具有差异性：枯水期河水呈Ca2+-HCO3-型；丰水期河流离子浓度受降水、冰川水的稀释影响离子浓度低，呈Ca2+-HCO3--SO42-型。（4）站点1到站点2河水中SO42-浓度突然升高，主要是由于此段河水的含水层中分布有石膏夹层，石膏夹层释放了大量硫酸和氯酸。（5）通过对地表水水化学过程的分析显示控制流域地表水化学过程的主要影响因素为水岩交互运动。
- Abstract:
- Based on the results of water chemistry of six stations in Urumqi River Basin in different seasons of 2011—2013, we analyzed the temporal and spatial characteristics of surface water chemistry in Urumqi River Basin by using water chemistry analysis method and SPSS statistical software in combination with hydrological data. The results show that: (1) the TDS of Urumqi River is lower and the water is slightly alkaline; (2) water hydrochemical characteristics varied over the years, TDS is lower in summer than that in early spring, early summer and autumn; (3) the control ions of the surface water are HCO3-, Ca2+, SO42-, the icon concentrations decrease in the order: HCO3- > Ca2+ > SO42- > Cl- > Na+ > Mg2+ > K+ > CO32-; the main ions changed with years: Ca2+ and HCO3 are the main ions in dry season; while Ca2+, HCO3 and SO42- start to dominate in wet season for the dilution of abundant water; (4) the SO42- concentration suddenly rises in site 1 to site 2 due to the release of sulfuric acid and chloric acid in the gypsum horizon of the river segment; (5) the conclusion indicates that water-rock interaction movement is the main factor controlling the surface water hydrochemical properties.
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备注/Memo
收稿日期:2016-11-21;改回日期:2017-01-21。
基金项目:中国博士后科学基金资助项目（2016M590989）；支持“率先行动”中国博士后科学基金会与中国科学院联合资助优秀博士后项目（2015LH048）；中国科学院农业水资源重点实验室开放基金（KFKT201601）
作者简介:吴丽娜(1992-),女,山西吕梁人,硕士研究生,研究方向为水化学。E-mail:sxwlina@sina.com
通讯作者:孙从建(1986-),男,河北沧州人,博士(后),主要从事水循环及同位素水文研究。E-mail:suncongjian@sina.com